一个超缓慢扩散的类型的海洋山脊
Henry J B Dick1, Jian Lin, Hans Schouten
1Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA. hdick@whoi.edu
Nature
|December 4, 2003
概括
新的研究确定了超缓慢扩散的海洋脊,与缓慢扩散的类型不同,具有连续的地幔安置和独特的amagmatic段. 这些发现重新定义了我们对板块边界结构的理解.
科学领域:
- 地质地质地质地质地质地
- 地质物理学 地质物理学
- 海洋学 海洋学 海洋学
背景情况:
- 海洋山脊对于理解板块构造学至关重要.
- 现有的分类区分快速,中等和缓慢扩散的山脊.
- 超缓慢扩散的山脊代表了以前未被充分描述的类别.
研究的目的:
- 为了研究超慢传播的海洋山脊的特征.
- 识别和描述与超慢传播相关的新型板块边界结构.
- 为了比较超慢传播的山脊与其他传播速率类.
主要方法:
- 印度西南部和北极山脊的地球物理调查.
- 对海底扩散过程的分析.
- 磁性和磁性脊段的映射. 磁性和磁性脊段的映射.
主要成果:
- 识别了一种独特的超慢传播海洋脊 (<20毫米/年) 类别.
- 发现连续地幔沉积到海底的发现.
- 鉴定amagmatic段作为一种新型的增积板边界结构的特征.
- 观察了岩层和岩层间的稳定共存和动态相互作用.
结论:
- 超慢传播的山脊表现出独特的地质特征和过程.
- 亚马格力细分代表了板块边界的重要,以前未被识别的组成部分.
- 超缓慢传播的动态与缓慢传播不同,因为缓慢传播与快速传播不同.
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